A transient ice sheet model simulation of the past 3 million years suggests that the Antarctic Ice Sheet became more sensitive to decreasing CO2 levels following the Mid-Pleistocene Transition, driven by the increasing influence of global sea-level changes…
Source: Nature Geoscience | Springer Nature Limited
Nature Geoscience | Springer Nature Limited
- Increased sensitivity of the Antarctic Ice Sheet to decreasing CO<sub>2</sub> across the Mid-Pleistocene Transition
- Diminished Ross Ice Shelf and West Antarctic Ice Sheet during Last Interglacial warming
- Precipitation threshold-driven shifts in dominant controls of ecosystem nitrogen retention
- Reduction of tropical cyclone-induced ocean carbon outgassing since 1993
- Viral mediation of anaerobic methane oxidation to carbon sequestration in paddy soil
- The global distribution of CO<sub>2</sub>-rich magmas is determined by lithospheric thickness
- Widespread peat carbon losses driven by the 2025 Scottish megafire
- Evapotranspiration declines prolonged by deforestation and fire in South American biomes
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